Minerals ROCK! This presentation was made possible with funding from the PromoScience programme of NSERC
|
|
|
- Winfred Gibbs
- 7 years ago
- Views:
Transcription
1 Minerals ROCK! This presentation was made possible with funding from the PromoScience programme of NSERC
2 Minerals Why are they important?
3 Minerals are important because: We use them in everyday life! Glass (Quartz)
4 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite)
5 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite) Toothpaste (Fluorite) and Public domain.
6 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite) Toothpaste (Fluorite) Coins and wiring (Chalcopyrite, from which most copper metal is made) and Public domain.
7 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite) Toothpaste (Fluorite) Coins and wiring (Chalcopyrite, from which most copper metal is made) White paint (Rutile and Ilmenite) and Public domain.
8 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite) Toothpaste (Fluorite) Coins and wiring (Chalcopyrite, from which most copper metal is made) White paint (Rutile and Ilmenite) Make-up (Talc, Muscovite) and wpclipart.com. Public domain.
9 Minerals are important because: We use them in everyday life! Glass (Quartz) Lead in pencil (Graphite) Toothpaste (Fluorite) Coins and wiring (Chalcopyrite, from which most copper metal is made) White paint (Rutile and Ilmenite) Makeup (Talc, Muscovite) Jewellery (Gold, Silver, Platinum ) and wpclipart.com. Public domain.
10 Minerals How many minerals are there in the world? Over 4200 different minerals! But only 100 are common Ones that are more rare include: Gold Public domain. Silver
11 What is a mineral? A mineral must have A crystalline structure A definite chemical composition A mineral must be Formed by geological processes Inorganic Solid
12 What does this mean? A mineral must have. A crystalline structure Minerals are made of molecules, and a crystalline structure is a repeated pattern of those molecules.
13 Crystalline structure (i) The crystalline structure explains the geometric shapes that crystals take on when they grow under favourable conditions.
14 Crystalline structure (ii) Crystals will keep growing
15 Crystalline structure (iii) and growing forever, as long as they have the chemical elements and the environmental conditions necessary.
16 Minerals are formed by geological processes They can t be man-made so steel is not a mineral. Public domain.
17 Minerals are inorganic Not living and not made by living things. Shells are not a type of mineral but they they are made of solid materials (biominerals) similar to some inorganic minerals. Redpath Museum
18 A mineral is solid Minerals may be dissolved in liquids but they themselves are not liquid.
19 Is ice a mineral? (i) Public domain.
20 Is ice a mineral? (ii) YES!! Inorganic Solid Crystalline structure As long as it is naturally occurring, ice is considered a mineral. Ice in your ice-cube tray is not naturally occurring: ice in a glacier is. Creative Commons Attribution-Share Alike 3.0 Unported license
21 Is water a mineral? (i) Public domain.
22 Is water a mineral? (ii) NO! Inorganic Naturally occurring But it is a LIQUID and has NO CRYSTALLINE STRUCTURE Public domain.
23 How are minerals formed? Many minerals crystallize from liquids, principally magma/lava (molten rock), hot waters (e.g., geysers), or oceans. Others are formed when rocks are re-buried below the Earth s surface and exposed to high pressure and temperature. The minerals become unstable and they exchange chemical elements. This forms new minerals.
24 Why are minerals found in large quantities in some places and not others? The Earth s surface is made up of plates that move. Plate tectonics describe this motion. Together with erosion, plate tectonics concentrate some of these elements in bodies of rocks that can be mined. Plate tectonics are the Earth's giant "recycling engine.
25 Plate tectonics Public domain.
26 The world s main plates Public domain.
27 Types of plate boundaries (i) Transform boundaries: plates grind past each other along a transform fault (e.g. San Andreas fault). public domain or licensed under a Creative Commons Attribution Share-Alike 3.0 License
28 Types of plate boundaries (ii) Divergent boundaries: plates slide away from each other (e.g., mid-oceanic ridges). Wikipedia.org, NASA: public domain
29 Types of plate boundaries (iii) Convergent boundaries: plates slide towards each other. If one plate moves underneath the other, it forms a subduction zone. Deep marine trenches, volcanoes, and some mountain chains (e.g., the Andes) form in these areas. Caribbean plate The Puerto Rico trench. Wikipedia.org, USGS: public domain North American plate
30 Types of plate boundaries (iv) Convergent boundaries (cont d): If the two plates collide and both contain continental crust, they form a continental collision. Some mountains (e.g., the Himalayas) form this way. Wikipedia.org, USGS: public domain
31 Rocks Public domain.
32 Rocks Rocks are made of minerals Granite is a rock made up of three main minerals: Feldspar Quartz Mica
33 A world of rocks There are 3 main types of rocks: Igneous rocks Metamorphic rocks Sedimentary rocks and Public domain. Redpath Museum
34 Igneous rocks Deep in the earth the temperatures are so high that materials, including minerals, melt and form magma. When the magma cools, it becomes rock. E.g., granite, basalt. Public domain.
35 Metamorphic rocks (i) When rocks are re-buried below the Earth s surface and exposed to high pressure and temperature, the minerals become unstable and they exchange chemical elements. This forms new minerals. This may also cause some grains to grow and others to shrink.
36 Metamorphic rocks (ii) This process produces new types of rocks that are different in composition and texture from the originals. E.g., bands of minerals are folded in gneiss. Gneiss Public domain. Slate
37 Sedimentary Rocks Sediments come from the erosion of previously existing rocks, dissolved minerals that precipitate out of solution, or the remains of plants and animals. Loose sediment accumulates in beds and, over time, becomes compressed and cemented together. These types of rocks are usually layered. E.g., limestone and sandstone. Sandstone Public domain. 2 Redpath Museum. Limestone 2
38 The Rock Cycle: Always Recycling 1. Magma 2. Crystallization 3. Igneous rock 4. Erosion 5. Sedimentation 6. Sedimentary rock 7. Tectonic burial 8. Metamorphic rock 9. Melting of rock and minerals Public domain.
39 Crystals Quartz Halite
40 What is the difference between minerals, crystals, and rocks? (i) Minerals are made up of regularly arranged atoms. Minerals grow as distinct objects called crystals. Agate (a form of the mineral quartz)
41 What is the difference between Crystals minerals, crystals, and rocks? (ii) Crystals are made up of only one type of mineral. A crystal s atoms, ions, or molecules are arranged in an orderly, repeating pattern. Crystals can have different shapes, depending on how the groups of atoms are arranged. Quartz crystal and penny
42 What is the difference between Crystals minerals, crystals, and rocks? (iii) A rock is a mass of many crystals from one or several minerals. Granite is a rock made of 3 main minerals: Feldspar Quartz Mica
43 How are crystals formed? Most come from a liquid evaporating (e.g., salt) or magma cooling. Minerals in the liquid precipitate out as the liquid evaporates. As more minerals precipitate out, the crystal grows in size. Crystals can grow forever, as long as they have the chemical elements and the environmental conditions necessary.
44 Mineral Identification (i) The two most important properties that scientists use to identify minerals are: chemical composition (e.g., via microprobe analysis) crystal structure (e.g., via X-ray diffraction analysis), which is reflected in the mineral's crystal symmetry and shape
45 Mineral Identification (ii) Other properties that scientists use to help identify minerals include: Colour Luster (how the surface reflects light) Streak (the mark it leaves on a ceramic plate) Hardness Magnetism Crystal system (crystal shape and the way in which the crystals are arranged)
46 Acknowledgments Scientific consultation Dr. Jeanne Paquette (Earth and Planetary Sciences) Dr. Peter Tarassoff (Redpath Museum) Concept, design, and production: Jacky Farrell Elizabeth Miazgy This presentation was made possible with funding from the PromoScience programme of NSERC
Rocks & Minerals. 10. Which rock type is most likely to be monomineralic? 1) rock salt 3) basalt 2) rhyolite 4) conglomerate
1. Of the Earth's more than 2,000 identified minerals, only a small number are commonly found in rocks. This fact indicates that most 1) minerals weather before they can be identified 2) minerals have
Rocks & Minerals 1 Mark Place, www.learnearthscience.com
Name: KEY Rocks & Minerals 1 KEY CONCEPT #1: What is a mineral? It is a naturally occurring, inorganic substance which has a definite chemical composition What would be the opposite of this? man-made,
Unit 4: The Rock Cycle
Unit 4: The Rock Cycle Objective: E 3.1A Discriminate between igneous, metamorphic, and sedimentary rocks and describe the processes that change one kind of rock into another. E 3.1B Explain the relationship
What are Rocks??? Rocks are the most common material on Earth. They are a naturally occurring collection of one or more minerals.
The Rock Cycle What are Rocks??? Rocks are the most common material on Earth. They are a naturally occurring collection of one or more minerals. The Rock Cycle a cycle that continuously forms and changes
What is a rock? How are rocks classified? What does the texture of a rock reveal about how it was formed?
CHAPTER 4 1 The Rock Cycle SECTION Rocks: Mineral Mixtures BEFORE YOU READ After you read this section, you should be able to answer these questions: What is a rock? How are rocks classified? What does
Earth Science Grade 4 Minerals
Earth Science Grade 4 Minerals Standards: Identifies the physical properties of minerals Teacher Background Minerals are pure substances and mix together to make rocks. Rocks have a cycle and different
How can you tell rocks apart?
How can you tell rocks apart? Grade Range: 4-7 G.L.E Focus: 1.1.5 Time Budget: 1 1.5 hours WASL Vocabulary: Overview: Different rocks have different characteristics because of their minerals, the ways
Rocks and Plate Tectonics
Name: Class: _ Date: _ Rocks and Plate Tectonics Multiple Choice Identify the choice that best completes the statement or answers the question. 1. What is a naturally occurring, solid mass of mineral or
Name: Rocks & Minerals 1 Mark Place, www.learnearthscience.com
Name: Rocks & Minerals 1 KEY CONCEPT #1: What is a mineral? It is a, substance which has a What would be the opposite of this? KEY CONCEPT #2: What causes minerals to have different physical properties?
1. Base your answer to the following question on on the photographs and news article below. Old Man s Loss Felt in New Hampshire
UNIT 3 EXAM ROCKS AND MINERALS NAME: BLOCK: DATE: 1. Base your answer to the following question on on the photographs and news article below. Old Man s Loss Felt in New Hampshire FRANCONIA, N.H. Crowds
Name: Class: Date: Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.
Class: Date: Minerals Study Guide Modified True/False Indicate whether the sentence or statement is true or false. If false, change the identified word or phrase to make the sentence or statement true.
Unit 8.3.1 Study Guide: Rocks, Minerals, and the Rock Cycle
Name Date Per Unit 8.3.1 Study Guide: Rocks, Minerals, and the Rock Cycle I Can Statements I Can Statements are the learning targets for each unit. By the time you take the test for this unit, you should
Grade 9 Geography - Unit 3 Lesson 3 The Rock Cycle
Grade 9 Geography - Unit 3 Lesson 3 The Rock Cycle What is the difference between a Rock and a Mineral? Minerals are homogeneous, naturally occurring, inorganic solids. Each mineral has a definite chemical
Rocks and Minerals What is right under your feet?
Rocks and Minerals What is right under your feet? Name: 1 Before you start What do you already know? What is the difference between a rock and a mineral? What are the three categories of rocks? 1. 2. 3.
EARTH SCIENCE 110 INTRODUCTION to GEOLOGY MINERALS & ROCKS LABORATORY
EARTH SCIENCE 110 INTRODUCTION to GEOLOGY DR. WOLTEMADE NAME: SECTION: MINERALS & ROCKS LABORATORY INTRODUCTION The identification of minerals and rocks is an integral part of understanding our physical
TECTONICS ASSESSMENT
Tectonics Assessment / 1 TECTONICS ASSESSMENT 1. Movement along plate boundaries produces A. tides. B. fronts. C. hurricanes. D. earthquakes. 2. Which of the following is TRUE about the movement of continents?
The rock cycle. Introduction. What are rocks?
The rock cycle This Revision looks at the three types of rock: sedimentary, igneous and metamorphic. It looks at how they are formed, the weathering of rocks and the way one form of rock turns into another,
Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: Geology: Inside the Earth (Approximate Time: 7 Weeks)
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
TYPES OF ROCKS & THE ROCK CYCLE
Visit http://www.learner.org/interactives/rockcycle/index.html to complete the following questions and activities. TYPES OF ROCKS: 1. Click on TYPES OF ROCKS. Read the information on the webpage and answer
Metamorphic rocks are rocks changed from one form to another by intense heat, intense pressure, and/or the action of hot fluids.
Metamorphic Rocks, Processes, and Resources Metamorphic rocks are rocks changed from one form to another by intense heat, intense pressure, and/or the action of hot fluids. Protolith or parent rock is
1. You are about to begin a unit on geology. Can anyone tell me what geology is? The study of the physical earth I.
PLATE TECTONICS ACTIVITY The purpose of this lab is to introduce the concept of plate tectonics and the formation of mountains. Students will discuss the properties of the earth s crust and plate tectonics.
1 Exploring Earth s Interior
1 Exploring Earth s Interior Crust Mantle Outer Core Crust-to-Mantle Inner Core Cross Section From Surface to Center SCIENCE EXPLORER Focus on Earth Science Prentice-Hall, Inc. 2 Evidence for Continental
II. Earth Science (Geology) Section (9/18/2013)
EAPS 100 Planet Earth Lecture Topics Brief Outlines II. Earth Science (Geology) Section (9/18/2013) 1. Interior of the Earth Learning objectives: Understand the structure of the Earth s interior crust,
ES Chapter 10 Review. Name: Class: Date: Multiple Choice Identify the choice that best completes the statement or answers the question.
Name: Class: Date: ES Chapter 10 Review Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Scientists used the pattern of alternating normal and reversed
Ch6&7 Test. Multiple Choice Identify the choice that best completes the statement or answers the question.
Ch6&7 Test Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Which of the following does NOT change the form of existing rock? a. tremendous pressure c.
Plate tectonics states that the Earth's crust and upper mantle are broken into sections, called plates.
Notes on Plate Tectonics Plate tectonics states that the Earth's crust and upper mantle are broken into sections, called plates. These plates move around the mantle. Plates are composed of the crust and
Earth Materials: Intro to rocks & Igneous rocks. The three major categories of rocks Fig 3.1 Understanding Earth
Earth Materials: 1 The three major categories of rocks Fig 3.1 Understanding Earth 2 Intro to rocks & Igneous rocks Three main categories of rocks: Igneous Sedimentary Metamorphic The most common minerals
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FOURTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FOURTH GRADE VOLCANOES WEEK 1. PRE: Comparing different structures of volcanoes. LAB: Modeling three types
3. Practice describing and classifying rocks as sedimentary, metamorphic or igneous.
Science Unit: Lesson 3: Renewable & Non-renewable Resources Mining in BC School Year: 2009/20010 Developed for: Developed by: Grade level: Duration of lesson: Notes: Dr. R. E. McKechnie Elementary School,
Plate Tectonics Web-Quest
Plate Tectonics Web-Quest Part I: Earth s Structure. Use the following link to find these answers: http://www.learner.org/interactives/dynamicearth/structure.html 1. Label the layers of Earth in the diagram
Characteristics of Sedimentary Rocks
Characteristics of Sedimentary Rocks Deposited at the earth s surface by wind, water, glacier ice, or biochemical processes Typically deposited in strata (layers) under cool surface conditions. This is
Interactive Plate Tectonics
Interactive Plate Tectonics Directions: Go to the following website and complete the questions below. http://www.learner.org/interactives/dynamicearth/index.html How do scientists learn about the interior
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SECOND GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SECOND GRADE VOLCANOES WEEK 1. PRE: Investigating the parts of a volcano. LAB: Comparing the parts of a
FROM SEDIMENT INTO SEDIMENTARY ROCK. Objectives. Sediments and Sedimentation
FROM SEDIMENT INTO SEDIMENTARY ROCK Objectives Identify three types of sediments. Explain where and how chemical and biogenic sediments form. Explain three processes that lead to the lithification of sediments.
Igneous Rocks. Geology 200 Geology for Environmental Scientists
Igneous Rocks Geology 200 Geology for Environmental Scientists Magma Compositions Ultramafic - composition of mantle Mafic - composition of basalt, e.g. oceanic crust. 900-1200 o C, 50% SiO 2 Intermediate
FIRST GRADE ROCKS 2 WEEKS LESSON PLANS AND ACTIVITIES
FIRST GRADE ROCKS 2 WEEKS LESSON PLANS AND ACTIVITIES ROCK CYCLE OVERVIEW OF FIRST GRADE CHEMISTRY WEEK 1. PRE: Comparing solids, gases, liquids, and plasma. LAB: Exploring how states of matter can change.
Assessment Plan for Geology 101 Lab (Online)
Plan for Geology 101 Lab (Online) John Turbeville, Earth Sciences MiraCosta College Description of course: This is an optional companion laboratory course for Geology 101, which is a survey level class.
4. Plate Tectonics II (p. 46-67)
4. Plate Tectonics II (p. 46-67) Seafloor Spreading In the early 1960s, samples of basaltic ocean crust were dredged up from various locations across the ocean basins. The samples were then analyzed to
All sediments have a source or provenance, a place or number of places of origin where they were produced.
Sedimentary Rocks, Processes, and Environments Sediments are loose grains and chemical residues of earth materials, which include things such as rock fragments, mineral grains, part of plants or animals,
6.E.2.2 Plate Tectonics, Earthquakes and Volcanoes
Name: Date: 1. The road shown below was suddenly broken by a natural event. 3. The convergence of two continental plates would produce Which natural event most likely caused the crack in the road? island
Chapter 8: Plate Tectonics -- Multi-format Test
Name: Class: Date: ID: A Chapter 8: Plate Tectonics -- Multi-format Test Modified True/False Indicate whether the statement is true or false. If false, change the identified word or phrase to make the
Three Main Types of Rocks Igneous Rocks. Sedimentary Rocks Metamorphic Rocks. Made by Liesl at The Homeschool Den
Three Main Types of Rocks Igneous Rocks Sedimentary Rocks Metamorphic Rocks Igneous Rocks Above and below: Basalt Above: Gabbro Above: Pumice Above: Basalt, Giant Causeway in Ireland Above: Obsidian Above:
Recommended Group Size: Groups of 2-3 This is a wet experiment and should ideally be done in the Science Lab
Grade: 3rd Activity #: 1 Activity Title: Studying Rocks and Minerals Recommended Group Size: Groups of 2-3 Special Notes: This is a wet experiment and should ideally be done in the Science Lab Purpose
Rock Identification Lab
Rock Identification Lab Name Mineral Hardness Objective: You will determine the relative hardness of common objects relative to the known hardness of index minerals. We will use fingernail, copper, glass,
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics. Wegener in Greenland about 1912. He froze to death there in 1930.
Alfred Wegener s Theory of Continental Drift Became Modern Plate Tectonics Wegener in Greenland about 1912. He froze to death there in 1930. Science is self correcting. The Scientific Method The history
EXPLORATION AND DISCOVERY IN PLANETARY SCIENCE
Rocks and Minerals I. OBJECTIVES One of the many ways to study Earth is by examining the rocks that make up its surface. Earth is a dynamic planet, with plate tectonics, water, wind, volcanoes, and mountains.
Chesapeake Bay Governor School for Marine and Environmental Science
Choose the best answer and write on the answer sheet provided. 1. Which of the following is LEAST likely to be an effect of global warming? (a) Loss of fertile delta regions for agriculture (b) Change
P1: Rock identification (I)
P1: Rock identification (I) Examine the rocks specimens provided with the aid of these notes. All the rocks come from Ireland, as detailed on the attached map. Answer the short question on each specimen
Regents Questions: Plate Tectonics
Earth Science Regents Questions: Plate Tectonics Name: Date: Period: August 2013 Due Date: 17 Compared to the oceanic crust, the continental crust is (1) less dense and more basaltic (3) more dense and
Georgia Performance Standards Framework for Shaky Ground 6 th Grade
The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are
FIFTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
FIFTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF FIFTH GRADE VOLCANOES WEEK 1. PRE: Exploring the rocks produced by volcanoes. LAB: Comparing igneous rocks.
Sedimentary Rocks. Find and take out 11B-15B and #1 From Egg Carton
Sedimentary Rocks Find and take out 11B-15B and #1 From Egg Carton Erosion Erosion is a natural process where rocks and soil are Broken and Moved We will focus on 4 types of erosion; Wind, Rain, Ice and
Rocks and Minerals Multiple Choice
Rocks and Minerals Multiple Choice 1. The basaltic bedrock of the oceanic crust is classified as (1) felsic, with a density of 2.7 g/cm3 (2) felsic, with a density of 3.0 g/cm3 (3) mafic, with a density
Atoms and Elements. Atoms: Learning Goals. Chapter 3. Atoms and Elements; Isotopes and Ions; Minerals and Rocks. Clicker 1. Chemistry Background?
Chapter 3 Atoms Atoms and Elements; Isotopes and Ions; Minerals and Rocks A Review of Chemistry: What geochemistry tells us Clicker 1 Chemistry Background? A. No HS or College Chemistry B. High School
Earth Egg Model Teacher Notes
Ancient Greeks tried to explain earthquakes and volcanic activity by saying that a massive bull lay underground and the land shook when it became angry. Modern theories rely on an understanding of what
LESSON PLAN FOR ROCKS AND MINERALS. Episode Six 306 Street Science (Earth Science)
LESSON PLAN FOR ROCKS AND MINERALS Episode Six 306 Street Science (Earth Science) Science lessons come easily if you are along a stream bed or road cut. All around you are examples of sedimentary rocks,
Lesson 13: Plate Tectonics I
Standards Addressed Lesson 13: Plate Tectonics I Overview Lesson 13 introduces students to geological oceanography by presenting the basic structure of the Earth and the properties of Earth s primary layers.
Ride the Rock Cycle. Suggested Goals: Students will gain an understanding of how a rock can move through the different stages of the rock cycle.
Illinois State Museum Geology Online http://geologyonline.museum.state.il.us Ride the Rock Cycle Grade Level: 5 6 Purpose: To teach students that the rock cycle, like the water cycle, has various stages
Plate Tectonics. Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics. And I am Buddy Zed s mascot
Plate Tectonics Hi, I am Zed and I am going to take you on a trip learning about Plate Tectonics And I am Buddy Zed s mascot Continental Drift Alfred Wegener proposed that continents were not always where
Tectonic plates push together at convergent boundaries.
KEY CONCEPT Plates converge or scrape past each other. BEFORE, you learned Plates move apart at divergent boundaries In the oceans, divergent boundaries mark where the sea floor spreads apart On land,
BOWEN'S REACTION SERIES
BOWEN'S REACTION SERIES Purpose John J. Thomas Frequently, people cannot visualize the mineral associations that form the sequences of igneous rocks that you find in the earth's crust and what happens
Earthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel
Earthquakes and Plate Boundaries Deborah Jordan and Samuel Spiegel Jordan, Deborah and Spiegel, Samuel: Learning Research Development Center, University of Pittsburgh. Earthquakes and Plate Boundaries.
Investigation 1-Part 1: Investigating Mock Rocks. Geology: the scientific study of Earth s history and structure
Investigation 1-Part 1: Investigating Mock Rocks Geology: the scientific study of Earth s history and structure Geologist: a person who studies the Earth and the materials of which it is made Property:
How Did These Ocean Features and Continental Margins Form?
298 10.14 INVESTIGATION How Did These Ocean Features and Continental Margins Form? The terrain below contains various features on the seafloor, as well as parts of three continents. Some general observations
Earth Structure, Materials, Systems, and Cycles
Page 1 of 19 EENS 3050 Tulane University Natural Disasters Prof. Stephen A. Nelson Earth Structure, Materials, Systems, and Cycles This page last updated on 31-Aug-2016 Objectives Since this course is
Lecture 23: Terrestrial Worlds in Comparison. This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies.
Lecture 23: Terrestrial Worlds in Comparison Astronomy 141 Winter 2012 This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies. The small terrestrial planets have
Continental Drift. Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on:
Plate Tectonics and Continental Drift Continental Drift Alfred Wegener (1880-1930) Proposed that all of the continents were once part of a large supercontinent - Pangaea Based on: Similarities in shorelines
Fourth Grade Geology: The Earth and Its Changes Assessment
Fourth Grade Geology: The Earth and Its Changes Assessment 1a. What is the center layer of the Earth called? a. crust b. core c. mantle d. middle 1b. Label each layer of the Earth. 1c. What are the Earth
1. The diagram below shows a cross section of sedimentary rock layers.
1. The diagram below shows a cross section of sedimentary rock layers. Which statement about the deposition of the sediments best explains why these layers have the curved shape shown? 1) Sediments were
Weathering, Erosion, and Soils. Weathering and Erosion. Weathering and Erosion
Weathering, Erosion, and Soils 1 The Grand Canyon, a landscape shaped by weathering and erosion 2 Weathering vs. erosion Types of weathering Physical Chemical Rates of weathering and erosion Climate Rock
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II
Geol 101: Physical Geology PAST EXAM QUESTIONS LECTURE 4: PLATE TECTONICS II 4. Which of the following statements about paleomagnetism at spreading ridges is FALSE? A. there is a clear pattern of paleomagnetic
The Dynamic Crust 2) EVIDENCE FOR CRUSTAL MOVEMENT
The Dynamic Crust 1) Virtually everything you need to know about the interior of the earth can be found on page 10 of your reference tables. Take the time to become familiar with page 10 and everything
Exploring How Rocks Are Formed
Exploring How Rocks Are Formed Grade Level: 3-4 Purpose and Goals: In this lesson, students are introduced to the three types of rocks: igneous, sedimentary, and metamorphic. After receiving background
Earth Materials: Minerals. Mineral Properties. Mineral Properties. Some optical properties. Three general categories:
1 2 Earth Materials: Minerals What is a mineral? Properties/characteristics of different types of minerals Mineral structures and bonding Major categories of minerals Importance and uses of minerals What
Plate Tectonics Practice Questions and Answers Revised August 2007
Plate Tectonics Practice Questions and Answers Revised August 2007 1. Please fill in the missing labels. 2. Please fill in the missing labels. 3. How many large plates form the outer shell of the earth?
Plate Tectonics Chapter 2
Plate Tectonics Chapter 2 Does not include complete lecture notes. Continental drift: An idea before its time Alfred Wegener First proposed his continental drift hypothesis in 1915 Published The Origin
SIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
SIXTH GRADE PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF SIXTH GRADE VOLCANOES WEEK 1. PRE: Comparing the structure of different types of volcanoes. LAB: Plotting
Presents the. Rock Test Study Resource
Presents the Rock Test Study Resource Created by Simone Markus Published by EngLinks 1 Preface This is a free resource provided by EngLinks for students in APSC 151. This presentation is a supplementary
DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes
DYNAMIC CRUST: Unit 4 Exam Plate Tectonics and Earthquakes NAME: BLOCK: DATE: 1. Base your answer to the following question on The block diagram below shows the boundary between two tectonic plates. Which
Chapter 2. Plate Tectonics. Plate Tectonics: Learning Goals
Plate Tectonics Chapter 2 Interactions at depend on the direction of relative plate motion and the type of crust. Which kind of plate boundary is associated with Earthquake activity? A. Divergent Boundary
Unit 4 Lesson 2 Plate Tectonics. Copyright Houghton Mifflin Harcourt Publishing Company
Puzzling Evidence What evidence suggests that continents move? In the late 1800s, Alfred Wegener proposed his hypothesis of continental drift. According to this hypothesis, the continents once formed a
Instructor: Ms. Terry J. Boroughs Geology 305 INTRODUCTION TO ROCKS AND THE ROCK CYCLE
DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 INTRODUCTION TO ROCKS AND THE ROCK CYCLE Instructions: Read each question carefully before selecting the BEST answer Provide specific and detailed
[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics}
![[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics}](/thumbs/40/21755359.jpg "[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics}")
[Geology Layers of the Earth] [Basic: Grade 2-3] [Advanced: Grade 5: Introduction to Plate Tectonics} BACKGROUND Scientists and geologists have been able to do some drilling on Earth. They are also able
Volcanoes Erupt Grade 6
TEACHING LEARNING COLLABORATIVE (TLC) EARTH SCIENCE Volcanoes Erupt Grade 6 Created by: Debra McKey (Mountain Vista Middle School); Valerie Duncan (Upper Lake Middle School); and Lynn Chick (Coyote Valley
The Rock Cycle: Metamorphic, Sedimentary, and Igneous Rocks
The Rock Cycle: Metamorphic, Sedimentary, and Igneous Rocks Intended for Grade: 3 Subject: Science Description: This presentation teaches students about the properties and formation of each of the three
1. A student found a sample of a solid material that was gray, shiny and made of all the same material. What category does this sample best fit?
Grade 4 Standard 3 Unit Test A Earth Materials Multiple Choice 1. A student found a sample of a solid material that was gray, shiny and made of all the same material. What category does this sample best
Instructor: Ms. Terry J. Boroughs Geology 305 INTRODUCTION TO ROCKS AND THE ROCK CYCLE
DATE DUE: Name: Instructor: Ms. Terry J. Boroughs Geology 305 INTRODUCTION TO ROCKS AND THE ROCK CYCLE Instructions: Read each question carefully before selecting the BEST answer Provide specific and detailed
ROCKS OF THE GRAND CANYON BACKGROUND INFORMATION FOR DOCENTS
ROCKS OF THE GRAND CANYON BACKGROUND INFORMATION FOR DOCENTS There are three distinct types of rock. Igneous rocks. Igneous comes from the Greek word for fire. It is so hot deep in the Earth that rocks
Plate Tectonics Lab. Continental Drift. The Birth of Plate Tectonics
Plate Tectonics Lab Continental Drift Take a look at a globe sometime and observe the remarkable fit between South America and Africa. Could they have, in fact, been connected? During the 19th and early
Plate Tectonics. Introduction. Boundaries between crustal plates
Plate Tectonics KEY WORDS: continental drift, seafloor spreading, plate tectonics, mid ocean ridge (MOR) system, spreading center, rise, divergent plate boundary, subduction zone, convergent plate boundary,
Layers of the Earth and Plate Tectonics
Layers of the Earth and Plate Tectonics Objectives: explain various ways the earth can be changed by natural forces define the term Geology define the terms Crust, Mantle, Outer Core and Inner Core classify
Ocean Floor Continental Slope Begins at the Continental Shelf Very sharp drop to depths over 2 miles Covered with thick layers of sand, mud, and rocks
Ocean Floor Continental Shelf Begins at the shoreline Gently slopes underwater Average depth of 430 feet Thick layers of sand, mud, and rocks The beach is part of the Continental Shelf Ocean Floor Continental
Santillana Intensive English Levels 4-6
Santillana Intensive English Levels 4-6 California Science Content Standards Grades 4-6 Grade 4 Physical Sciences 1. Electricity and magnetism are related effects that have many useful applications in
KINDERGARTEN PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES
KINDERGARTEN PLATE TECTONICS 1 WEEK LESSON PLANS AND ACTIVITIES PLATE TECTONIC CYCLE OVERVIEW OF KINDERGARTEN VOLCANOES WEEK 1. PRE: Learning that all mountains are not volcanoes. LAB: Investigating rocks
Essential Standards: Grade 4 Science Unpacked Content
This document is designed to help North Carolina educators teach the Essential Standards (Standard Course of Study). NCDPI staff are continually updating and improving these tools to better serve teachers.
Plate Tectonics Short Study Guide
Name: Class: Date: Plate Tectonics Short Study Guide Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. The existence of coal beds in Antarctica
Geology Laboratory: Metamorphic Rocks
OBJECTIVES Learn to identify metamorphic rocks by structure and mineralogy. Identify major minerals contained within a metamorphic rock. Distinguish between foliated and non-foliated metamorphic rocks.
Igneous Geochemistry. What is magma? What is polymerization? Average compositions (% by weight) and liquidus temperatures of different magmas
1 Igneous Geochemistry What is magma phases, compositions, properties Major igneous processes Making magma how and where Major-element variations Classification using a whole-rock analysis Fractional crystallization
Layers of the Earth s Interior
Layers of the Earth s Interior 1 Focus Question How is the Earth like an ogre? 2 Objectives Explain how geologists have learned about the interior of the Earth. Describe the layers of the Earth s interior.
Name: Period: # Plate Tectonics. Journey to the center of the Earth
Plate Tectonics Journey to the center of the Earth Use pages 124 129 to answer the following questions. Exploring Inside Earth (p. 125-126) 1. What are the two main types of evidence that Geologist use